Why do we find evidence of strike-slip and normal-fault stress regimes in addition to the thrust-fault regime

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Why do we find evidence of strike-slip and normal-fault stress regimes in addition to the thrust-fault regime in active

(contractional) orogens such as the Himalaya and Andes?

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Related Book For  answer-question

Structural Geology

ISBN: 9781107057647

2nd Edition

Authors: Haakon Fossen

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